The 4th of July, the day of Mr. Weld's arrival at Albany, was the anniversary of the declaration of American independence. About noon a drum and trumpet gave notice that the rejoicings would immediately commence; and, on walking to a hill, about a quarter of a mile from the town, Mr. Weld saw sixty men drawn up, partly militia, partly volunteers, partly infantry, partly cavalry. The last were clothed in scarlet, and were mounted on horses of various descriptions. About three hundred spectators attended. A few rounds from a three-pounder were fired, and some volleys of small-arms. When the firing ceased, the troops returned to the town, a party of militia officers, in uniform, marching in the rear, under the shade of umbrellas, as the day was excessively hot. Having reached the town, the whole body dispersed. The volunteers and militia officers afterwards dined together, and thus ended the rejoicings of the day. Mr. Weld remained in Albany for a few days, and then set off for Skenesborough, upon Lake Champlain, in a carriage hired for the purpose. In about two hours he arrived at the small village of _Cohoz_, close to which is a remarkable cataract in the _Mohawk River_. This river takes its rise to the north-east of Lake Oneida, and, after a course of one hundred and forty miles, joins the Hudson about ten miles above Albany. The _Cohoz fall_ is about three miles from the mouth of this river, and at a place where its width is about three hundred yards: a ledge of rocks extends quite across the stream, and from the top of these the water falls about fifty feet perpendicular: the line of the fall, from one side of the river to the other, is nearly straight. The appearance of this cataract varies much, according to the quantity of water: when the river is full, the water descends in an unbroken sheet from one bank to the other; but, at other times, the greater part of the rocks is left uncovered. From this place Mr. Weld proceeded along the banks of the _Hudson River_, and, late in the evening, reached _Saratoga_, thirty-five miles from Albany. This place contained about forty houses; but they were so scattered, that it had not the least appearance of a town. Near Saratoga, on the borders of a marsh, are several remarkable mineral springs: one of these, in the crater of a rock, of pyramidical form, and about five feet in height, is particularly curious. This rock seems to have been formed by the petrifaction of the water; and all the other springs are surrounded by similar petrifactions.